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1.
大家盼望已久的《中华人民共和国海域使用管理法》（以下简称《海域法》）于２００１年１０月２７日由第九届全国人大常务委员会第２４次会议通过，并由中华人民共和国主席江泽民签署第６１号令颁布，自２００２年１月１日起施行，这是我国政府依法强化海洋综合管理的又一重大举措，是我国海洋法制化建设又一个重要里程碑，也是值得全国海洋战线隆重庆祝并欢欣鼓舞的一件大喜事！《海域法》的发布施行，不仅标志着我国海域使用管理工作开始走上依法用海、以法管海的新阶段，而且对于依法加大海域使用管理的力度，遏制海域使用无序、无度、无… 相似文献
2.
东台市位于江苏省中部的黄海之滨,水土肥沃、物产丰饶.21世纪之初,江苏省委、省政府以沿海开发为重点,作出了加快建设海上苏东的重大战略部署.百万东台人民乘风乘势,以贯彻实施《中华人民共和国海域使用管理法》、《江苏省海域使用管理条例》和《江苏省蒋家沙竹根沙海域管理暂行办法》为契机,以大力发展海水养殖业为重点,强化依法管海用海,注重科技兴海,坚持保护性开发利用,不断加快海洋经济开发步伐,使海洋经济发展取得了明显成效. 相似文献
3.
《中华人民共和国海域使用管理法》自2002年1月1日施行以来,已经五年了。今天,全国人大环境与资源保护委员会、国务院法制办公室、国家海洋局联合召开“纪念《海域使用管理法》实施5周年”座谈会,邀请有关部门、用海企业、大学和新闻媒体,共同回顾总结这部法律施行五年来的主要成绩和经验,意义重大。希望以此为契机,深入宣传贯彻《海域使用管理法》,为进一步规范海洋开发秩序、维护国家海域所有权和海域使用权人的合法权益,保障海洋经济持续健康发展创造良好的氛围和环境。 相似文献
4.
<正>近日,广饶县海域动态监控室终端完成,标志着广饶县科学用海、依法管海水平跃上一个新的台阶,广饶县海洋管理数字化、规范化、科学化、信息化水平进一步提高,促进了海洋的合理开发和海域 相似文献
5.
根据江苏省人民政府办公厅《关于对蒋家沙竹根沙海域实行省统一管理的通知》精神,江苏省海洋与渔业局于2006年3月10日在南京市成立了"江苏省蒋家沙竹根沙海域管理委员会"(以下简称"两沙"海管会),下设办公室挂靠在江苏省海洋渔业指挥部,具体负责"两沙"海域内的海洋与渔业行政管理工作,依法受理"两沙"海域渔业用海申请并进行审核.为平稳推进"两沙"海域重新确权工作,围绕"科学用海、团结管海、依法治海"三原则以及"科学用海的示范区、团结管海的和谐区、安全生产的放心区"的建设目标,我们要统一思想,强化管理,不断开创和谐"两沙"新局面. 相似文献
6.
《海域法》于2001年10月27日通过,并于2002年1月起开始实施,《海域法》的颁布实施是我国海洋管理法制建设中的一件大事。值此《海域法》颁布五周年之际,本刊将连续三期开设专栏集中报道海域管理工作的成效,广泛普及海域管理法律知识,推动物权立法工作,引导全社会依法用海,更好地为经济社会发展服务。 相似文献
7.
2011 年是《中华人民共和国海域使用管理法》（以下简称《海域法》）颁布十周年,十年来,在国家海洋局和省委、省政府的正确领导下,河北省以海洋功能区划、海域权属管理、海域有偿使用三项制度为核心,不断加大海域管理工作力度,不断提高依法行政水平,依法用海观念深入人心,海洋资源保障能力显著提高,海洋经济综合实力不断增强。 相似文献
8.
9.
《中华人民共和国海域使用管理法》(以下简称《海域法》)第三条规定,海域属于国家所有,国务院代表国家行使海域所有权。任何单位或个人不得侵占、买卖或者以其他形式非法转让海域。单位和个人使用海域,必须依法取得海域使用权。自《海域法》颁布实施以来,各项制度得到广泛实施,海域使用管理进一步规范、更趋科学合理。同时,配套的《海域使用管理技术规范》为界定项目用海范围,规范海域使用权的申请、办理、确权与管理提供了有力的技术支撑。但是,对有些功能使用上交叉的海域,或者同一海域不同空间上(水面、底土)使用的海域等特殊情况下如何… 相似文献
10.
盐城市作为国家第二批海域使用管理示范区，通过一年多的艰苦工作，取得了良好的成绩。全市共登记海域使用申请５３８份，登记使用海域面积３２０万多亩，海域使用登记率达１００％，完成了大比例尺功能区划的编制，起草了４个规范性文件，海域管理工作实现了明显转变：一是海域使用管理由有法不依、无序用海向科学管理、依法用海转变。《暂行规定》确定的两项制度已纳入规范化、法制化管理轨道，海域使用许可证制度基本建立。广大海域使用者根据需要，依法申请登记用海，初步改变了以往自由放任，擅自占用海域的现象；二是海域使用者初步树… 相似文献
11.
The analysis of the structure of the cryolithozone, facies, and thicknesses of the Quaternary sediments and the results of the physicochemical mathematical modeling of the modern shelf of the western part of the Laptev Sea support the influence of the Late Pleistocene glaciations on the heat conditions and the distribution of the permafrost in the area. A ～200-m thick glacier formed under aerial conditions from atmospheric precipitation represented the metamorphosed snow cover. According to the modeling, the long-living (from 60?50 to 10?4 ky) glacier reduced the thickness of the permafrost rocks in the reviewed shelf area for 280–360 m. The Holocene marine transgression additionally decreased the thickness from 50–140 m on the inner shelf to 220–350 m on the outer shelf. The modern submarine cryolithozone 450-0 m thick is wide-spread in the studied region from the coast to the shelf boundary (isobaths of 130–140 m), where it pinches out at a distance of ～380 km from the coast at a depth of ～250 m above the sea level. 相似文献
12.
We analyze the components of the carbon system of the Sevastopol bay waters and the balance of main sediment-forming substances
using the data of field investigations in 1998–2008. The interannual variations of total inorganic carbon and the equilibrium
partial pressure of carbon dioxide in the bay water are noted. An increase in the flux of carbon dioxide into the bay and
in the content of organic carbon in bottom sediments is revealed, and an explanation of this phenomenon is given. The priority
accumulation of organic carbon in the sediments of the bay is established. We assess the interannual variation in the relative
abundances of organic and inorganic carbon as an index of the carbon cycle stability. 相似文献
13.
We generalize and analyze the state of investigations of the influence of river waters on the hydrologic structure of the
Black Sea. Specific features of the water, regime and hydrography of rivers flowing into the sea, data on the discharge of
rivers, and intrayear and interyear variability of the discharge are presented. We discuss and analyze works studying the
transformation of river waters, routes of desalinized sea waters, and their influence on the thermohaline structure and dynamic
regime of the sea.
Translated by Peter V. Malyshev and Dmitry V. Malyshev 相似文献
14.
V. A. Ivanov S. P. Lyubartseva N. Mikhailova N. B. Shapiro 《Physical Oceanography》2001,11(6):509-524
We analyze the results of numerical calculations performed according to the three-dimensional interdisciplinary model of an
ecological system of the Black-Sea shelf zone near the estuary of the Danube. The complete system of equations of hydrothermodynamics
is solved together with transport equations of the advection-diffusion-reaction type used to describe the transformation of
a substance (nitrogen) between the components of the characteristic vectors of the ecosystem: plankton, detritus, and biogenic
elements (nitrates). We describe the distinctive features of the circumcontinental distribution of components obtained as
a result of numerical experiments and present arguments for the conclusion that the ecosystem of the Danube estuary water
area plays the role of a buffer zone between the press of the Danubian biogenic pollutions and the neighbouring areas of the
shelf zone and open sea.
Translated by Peter V. Malyshev and Dmitry V. Malyshev 相似文献
15.
Ten years of semistationary studies of the interaction of the ice cover and the coastal relief of the Kandalakhsa Gulf in the White Sea allowed us to reveal the peculiarities of these processes in the warm and cold years and the mechanisms of the origination of ice forms, including ice tents, which govern the character of the tidal flats. Three dynamic fast ice zones are distinguished by their geomorphological location, morphology, and ice dynamics. The dependence of the mechanisms and volumes of the enrichment of the fast ice in the sediments on the coastal zone??s relief was established. At the coast of the Kindo Peninsula (Velikaya Salma Strait), the ice mostly contains fine-sandy sediments. Coarser sediments, including boulders, are occasional and frozen into the ice at the contact of the fast ice and the bottom. At the expense of the ice??s spreading by 4?C6 times in the warm years and 2?C4 times in the cold years, several thousand tons of sediments mostly from the tidal flat??s surface (100?C700 m3 from 1 km of coast in the wide tidal flats and <50 m3 on the steep coasts) are delivered to the water area. 相似文献
16.
Relationship between the path of the Kuroshio in the south of Japan and the path of the Kuroshio Extension in the east 总被引：2，自引：0，他引：2
A relationship between paths of the Kuroshio and Kuroshio Extension (KE) is investigated, using the satellite-derived altimetry
dataset of 1993–2008. When the Kuroshio takes the nearshore nonlarge meander path or typical large meander path and resultantly
goes through the deeper channel (about 2500 m) of the Izu-Ogasawara Ridge, the KE path adopts a relatively stable state with
the two quasi-stationary meanders. On the other hand, when the Kuroshio takes the offshore nonlarge meander path and then
passes over the shallower part of the Ridge (about 1000 m), the KE path tends to be convoluted, i.e., an unstable state. 相似文献
17.
Izvestiya, Atmospheric and Oceanic Physics - Analysis of the temporal variations of the virtual heights of the sporadic E layer (h?ES) determined from ionograms with increased accuracy (1... 相似文献
18.
I. E. Timchenko A. A. Primalenny V. D. Yarin E. F. Vasechkina E. M. Igumnova 《Physical Oceanography》2001,11(4):367-378
We use many-year archival observations of hydrologic and hydrobiologic state of the Sea of Azov for the identification of
the structure of a model of its ecosystem. The ecosystem model, supplemented with expert estimates of bioresource consumption
(fish reserve), contamination level, and possible ecologic fines for violation of the sea natural state, is formalized by
the method of system dynamics. Hereat, the major part of influence functions is found in terms of observational data with
application of self-organization algorithms. We also present the results of simulated experiments with the model of the ecosystem,
which enable us to analyse scenarios of its behaviour under the influence of various external factors (wind, river discharge,
water exchange with the Black Sea, etc.).
Translated by Peter V. Malyshev and Dmitry V. Malyshev 相似文献
19.
The methodology and the first results of the computations of the volumes, masses, and growth rates of the sedimentary body of the buried Black Sea basin are presented. Their temporal evolution reflects the regional paleogeodynamics, in particular, the reorientation of the vector of the relative movement of the Arabian and Eurasian lithospheric plates and the related intensification of their collision in the late Miocene-Pliocene. 相似文献
20.
E. L. Vinogradova 《Oceanology》2008,48(4):483-492
The spatiotemporal variability of the hydrochemical composition of the riverine runoff in nearmouth areas is presented using the example of selected rivers of the Arctic Basin. The temporal dynamics of the riverine nutrient runoff are mainly determined by the seasonal and interseasonal variations in the drainage basins. The spatial variations in the chemical composition of riverine waters in the near-mouth areas are mainly caused by the dynamics of the water flow and the river bed relief and, to a lesser degree, by biochemical processes. It is shown that the variations in the nutrient composition of the waters in near-mouth areas are comparable in magnitude to those at the river-sea geochemical barriers. 相似文献